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相山火山盆地岩石稀土元素分布特征及其成因探讨
引用本文:窦小平. 相山火山盆地岩石稀土元素分布特征及其成因探讨[J]. 铀矿地质, 2005, 21(6): 338-344
作者姓名:窦小平
作者单位:江西省核工业地质局测试研究中心,江西,南昌,330002
摘    要:本文通过对相山火山盆地基底震旦系浅变质岩、盖层火山岩稀土元素分布特征的研究,探讨相山火山岩的物质来源及岩石成因,认为相山火山岩主要是上部地壳重熔的产物,其岩石成因应属于重熔型花岗岩的范畴。

关 键 词:相山火山盆地  震旦系浅变质岩  侏罗系火山岩  稀土元素特征  岩石成因
文章编号:1000-0658(2005)06-0338-07
收稿时间:2004-10-17
修稿时间:2004-10-17

REE distribution characteristics of volcanic and epimetamorphic rocks in Xiangshan volcanic basin and discussion on their genesis
DOU Xiao-ping. REE distribution characteristics of volcanic and epimetamorphic rocks in Xiangshan volcanic basin and discussion on their genesis[J]. Uranium Geology, 2005, 21(6): 338-344
Authors:DOU Xiao-ping
Affiliation:Testing and Research Center, Geologic Bureau of J iangxi Nuclear Industry, Nanchang , Jiangxi 330002, China
Abstract:Based on the study on REE distribution characteristics of Sinian low-grade metamorphic rocks of the basement and cover volcanics,the author makes a discussion on the material source and the gene-sis of Xiangshan volcanics,and suggests that Xiangshan volcanics came mostly from the remelting of the upper crust,and the genesis should be attributed to the category of remelted granites.
Keywords:Xiangshan volcanic basin  Sinian epimetamorphic rocks  Jurassic volcanics  REE character-istics  genesis of rocks
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